1958, 6(3):157-177.
Abstract:Почвенное районирование Китая было проведено как частъ работы комплексного природного районирования.
1958, 6(3):178-192.
Abstract:Clay particles of less than 1μ were separated from 18 selected soil samples,representing important types of red and yellow soils of southern China. Composition of clay minerals was identified by X-ray defraction, difFerential thermal analysis, base exchange capacity and chemical constituents. Zonality of the weathering stage of the soil, as shown in Fig. I, is explained briefly as follows.
1958, 6(3):193-204.
Abstract:关于热带地区的土壤,虽然积累有广泛的世界文献资料,但无论是在其发生方面,或是其受植被演替及其他因素影响的演变方面,都还很不清楚。原因是因为各国学者都片面地偏重于研究土壤的化学和矿物学,旨在阐明热带各种自然地理条件下成土母质的风化过程和风化阶段。
C. C. WANG , K. C. CHANG , S. M. VONG
1958, 6(3):205-208.
Abstract:A new method for complete analysis of soil colloid was proposed.The SiO2, content was determined by the loss of weight of HF-HN03 evaporation and ignition at 870-9000C for 30-40 minutes.
1958, 6(3):209-213.
Abstract:Сравнив некоторые методы определения,емкости поглощения катионов,мы считаем,что метод Е.В.Бобка(BaCl2-H2SO4) позволяет в сравнителъно болышом объеме правилвилъно определить емкость поглощения ионов почвы и глинистых минералов.
1958, 6(3):214-215.
Abstract:在过去三十年的土壤学教材中,对于酸性土壤(特别是红壤)的磷素固定作用异常强调,以为可溶性磷一经施入在强酸性土壤以后,大部分以铝铁磷酸盐沉澱,不能被植物所吸收。同时许多测定土壤有效性磷的方法,在应用于施有大量过磷酸钙的红壤标本上,也得不出有正面的结果。